Concept Studio

See the idea. Put it to the test.

956 activities from Kindergarten to Year 12, in 13 subject areas. A practical gives the idea, what you need, the steps, what you should see and a safety card. A teacher-led demonstration gives the idea and its hazards; its method is for tutors on the learning platform.

Review

Reviewed before publication (owner’s confirmation, 24 September 2026). That covers every activity here, and a practical’s page lists the sources its author read.

A safety card on every page

The risk, who supervises and the hazards. The 38 teacher-led demonstrations show their idea and hazards here; their materials, steps and sources, and any result, control or note that states a number or an amount, are for tutors and administrators on the learning platform.

School laboratory, not for home

207 activities are medium or high risk. Each says so on its page: In a school laboratory, with a teacher supervising, under the school's risk assessment. Not for home.

Curriculum references

Each activity lists the NSW syllabus outcomes and Australian Curriculum v9 codes it supports. They are references, not a verified or complete curriculum alignment.

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A practical is carried out at the bench, in the classroom or outdoors. A practical with its model not built stands on its own; the page says where a step mentions the model. A calculation and data activity works from published figures by hand, with a calculator or in a spreadsheet. No page includes an interactive model.

44 activities

Geography K–10

  1. Geography K–10 · Kindergarten

    Bird's-eye view: from a model of the classroom to a pictorial map

    A map shows places as they look from directly above, so objects keep their positions relative to each other when a room is drawn as a plan.

    PracticalLow risk
  2. Geography K–10 · Years 1–2

    A term of weather and nature records beside a published Aboriginal seasonal calendar

    Seasons can be read from plants, animals and weather in a place rather than from dates, and the Aboriginal calendar for a Country divides the year differently from the four-season calendar.

    PracticalLow risk
  3. Geography K–10 · Years 1–2

    Feature walk: natural, managed and constructed features on a labelled map

    Every feature of a local place can be sorted as natural, managed or constructed, and its position can be recorded on a map.

    PracticalLow risk
  4. Geography K–10 · Years 1–2

    How much water does our school use in a day

    Water use can be measured in litres with a bucket and a timer, and a day's total for a place is the sum of many small uses.

    Practical, model not builtLow risk
  5. Geography K–10 · Years 1–2

    Make a rain gauge and keep a monthly rainfall record

    Rainfall is a depth of water spread over the ground, so a straight-sided container measures it in millimetres regardless of the container width.

    Practical, model not builtLow risk
  6. Geography K–10 · Years 1–2

    Wind vane, compass and a class wind rose

    Wind has a direction that can be named by the compass point it comes from, and a month of daily readings shows which directions are most common at the school.

    PracticalLow risk
  7. Geography K–10 · Years 3–4

    Erosion trays: bare soil, mulched soil and turf under the same rain

    Plant cover and mulch slow water and hold soil, so the same rainfall carries far less soil off a covered slope than off a bare one.

    PracticalLow risk
  8. Geography K–10 · Years 3–4

    Measure the playground and draw it to scale

    A scale is a fixed ratio between map distance and ground distance, so measured ground lengths become map lengths by division.

    Practical, model not builtLow risk
  9. Geography K–10 · Years 3–4

    States, territories and neighbours on a real map, with scale-bar distances

    Australia and its neighbours are located by direction and distance, and a printed scale bar turns a string length into kilometres.

    Practical, model not builtLow risk
  10. Geography K–10 · Years 3–4

    Where is Earth's water: dividing one litre by the real proportions

    Almost all of Earth's water is sea water and most fresh water is ice or underground, so the water people draw from rivers and lakes is a tiny share.

    Practical, model not builtLow risk
  11. Geography K–10 · Years 5–6

    Catchment model: where the rain goes

    Rain that falls anywhere inside a catchment boundary drains to the same low point, carrying whatever is on the surface with it.

    PracticalLow risk
  12. Geography K–10 · Years 5–6

    Climate graphs for two Australian stations from Bureau data

    Two places at different latitudes have different patterns of monthly rainfall and temperature, and a climate graph makes the pattern comparable at a glance.

    PracticalLow risk
  13. Geography K–10 · Years 5–6

    Fire danger from the schoolyard: temperature, humidity and wind into the McArthur index

    Fire danger is set by weather that can be measured, and it rises steeply with heat and wind and falls with humidity, which is why the same bush can be safe one afternoon and dangerous the next.

    Practical, model not builtLow risk
  14. Geography K–10 · Years 5–6

    Latitude, longitude and the shortest route: string on a globe against a flat map

    Latitude and longitude fix any place on the globe, and the shortest route between two places is a great circle, which a string pulled tight on a globe follows and a straight line on a flat map does not.

    Practical, model not builtLow risk
  15. Geography K–10 · Years 5–6

    Read the bushfire prone land map around the school

    Bush fire prone land is mapped by local councils and certified by the Commissioner of the NSW Rural Fire Service, so the hazard around a place can be read from an official map and measured with its scale.

    PracticalLow risk
  16. Geography K–10 · Years 5–6

    Surface temperature survey of the schoolyard with an infrared thermometer

    Surface cover chosen by people (asphalt, concrete, grass, shade trees) sets how hot a surface becomes in the sun, which is the mechanism behind urban heat.

    PracticalLow risk
  17. Geography K–10 · Years 7–8

    Angle of repose: how steep a slope of loose material can stand

    Loose material piles up to a fixed maximum angle that depends on the grains and their wetness, and a slope cut steeper than that angle fails.

    PracticalMedium risk
  18. Geography K–10 · Years 7–8

    Aquifer in a tank: porosity, permeability and a pumped well

    Groundwater fills the pore space between grains; how much a layer holds is its porosity and how fast water moves through it is its permeability, and pumping a well lowers the water table around it.

    Practical, model not builtLow risk
  19. Geography K–10 · Years 7–8

    Contour lines from a model hill in a rising tank

    A contour is the line where a level surface meets the land, so raising water in fixed steps around a model hill draws the contour map of that hill.

    Practical, model not builtLow risk
  20. Geography K–10 · Years 7–8

    Creek discharge from a cross-section and float timing

    Discharge is cross-sectional area multiplied by velocity, so a creek's flow in litres per second can be measured with a tape, a ruler and a floating orange.

    Practical, model not builtMedium risk
  21. Geography K–10 · Years 7–8

    Dune formation: wind over bare and planted sand

    Wind moves dry sand grains and drops them where the wind slows, so any obstacle including plants starts a dune and holds it.

    PracticalMedium risk
  22. Geography K–10 · Years 7–8

    How much rain does the roof catch: from gauge depth to tank litres

    Rainfall depth times catchment area gives a volume, so a school roof and a rain gauge reading predict the litres a tank receives from one storm.

    Practical, model not builtLow risk
  23. Geography K–10 · Years 7–8

    Liveability transect: measuring environmental quality at five sites

    Environmental quality can be measured, not only felt: noise, shade, litter, traffic and surface heat differ along a walk through a suburb and can be scored and mapped.

    PracticalLow risk
  24. Geography K–10 · Years 7–8

    Locating an earthquake from P and S wave arrival times

    P waves outrun S waves, so the gap between their arrivals at a station gives the distance to the earthquake, and three distances fix the epicentre.

    Practical, model not builtLow risk
  25. Geography K–10 · Years 7–8

    Longshore drift in a wave tray, with and without a groyne

    Waves that arrive at an angle carry sand along the beach in the direction they travel, and a wall built across the beach traps sand on the side the sand comes from and starves the other side.

    Practical, model not builtLow risk
  26. Geography K–10 · Years 7–8

    Reading a real topographic map: grid references, distance, area and gradient

    A topographic map encodes position, distance, area and height in a fixed grid, scale and contour interval, so real landform sizes and slopes can be computed from it.

    Practical, model not builtLow risk
  27. Geography K–10 · Years 7–8

    Ring infiltrometer: how fast water soaks into three surfaces

    Infiltration rate falls as the soil wets up and differs by surface, which decides how much rain becomes runoff instead of soil water.

    Practical, model not builtLow risk
  28. Geography K–10 · Years 7–8

    Storm hydrograph from a stream table: bare catchment versus sponge wetland

    A catchment turns a short burst of rain into a longer, lower outflow, and storage on the surface (vegetation, wetlands) lengthens the delay and lowers the peak, which is what reduces flooding downstream.

    Practical, model not builtLow risk
  29. Geography K–10 · Years 7–8

    Stream table: meanders, cut banks, point bars and a delta

    Flowing water erodes where it moves fastest (outside of bends) and deposits where it slows (inside of bends and at the mouth), so a straight channel becomes a meandering one and builds a delta.

    PracticalLow risk
  30. Geography K–10 · Years 7–8

    Tectonic plates on a tennis ball and how far Australia moves

    The rigid outer shell of the Earth is the lithosphere, the crust together with the strong uppermost mantle, and it is broken into plates that move over the weaker rock below; their edges are where earthquakes, volcanoes and mountain building happen, and their motion is slow but measurable.

    Practical, model not builtLow risk
  31. Geography K–10 · Years 7–8

    Waterwatch water quality testing of a local waterway

    The health of a waterway is measured by a fixed set of physical and chemical readings plus the animals living in it, compared against published guideline ranges.

    PracticalMedium risk
  32. Geography K–10 · Years 7–8

    Weathering: freeze–thaw on wet sandstone and acid on chalk

    Rock is broken down in place by physical stress (water expanding as it freezes) and by chemical reaction (acid dissolving calcium carbonate), and both can be measured as mass lost.

    PracticalLow risk
  33. Geography K–10 · Years 7–8

    Where our things come from: a label survey and a flow-line map

    Everyday goods connect a household to producing places around the world, and counting labels and drawing flow lines with measured widths turns that connection into a map.

    Practical, model not builtLow risk
  34. Geography K–10 · Years 7–8

    Who lives within walking distance: buffers around services on a scaled map

    Access to a service depends on distance, and a circle of fixed ground radius drawn to the map scale shows which homes are within that straight-line distance of it, which is not the same as being within that walking distance.

    Practical, model not builtLow risk
  35. Geography K–10 · Years 9–10

    Beach profile survey with two graduated poles and the horizon (Emery method)

    A beach's shape changes with waves and storms, and repeated profiles along a fixed line measure where sand has been lost or gained and by how much.

    Practical, model not builtMedium risk
  36. Geography K–10 · Years 9–10

    Computing the Human Development Index from its four indicators

    Human development is measured by combining health, education and income indicators, each scaled between fixed goalposts and joined by a geometric mean, so a country cannot make up for a very low score in one dimension with a high score in another.

    Calculation and dataLow risk
  37. Geography K–10 · Years 9–10

    How fast is this beach moving: shoreline change from annual satellite shorelines

    Annual shorelines mapped from satellite imagery since 1988 show whether a coast is eroding or growing, and a line fitted through the positions gives the rate in metres per year.

    Practical, model not builtLow risk
  38. Geography K–10 · Years 9–10

    How much wheat can the rain grow: the French and Schultz potential yield model

    In a dryland wheat biome the growing-season rainfall sets a ceiling on grain yield, because a fixed amount of water is lost from the soil surface before the crop can turn water into grain.

    Calculation and dataLow risk
  39. Geography K–10 · Years 9–10

    Mapping advantage and disadvantage: a choropleth from ABS SEIFA scores

    Wellbeing varies across places within Australia, and a choropleth map of an index shows the pattern, but the classes chosen for the map change what the pattern appears to be.

    Practical, model not builtLow risk
  40. Geography K–10 · Years 9–10

    Measuring urban growth with a grid over annual satellite composites

    Urban growth can be measured, not just described, by counting grid cells of built-up land in satellite images of the same frame from two years.

    PracticalLow risk
  41. Geography K–10 · Years 9–10

    Population pyramid from Census data and a growth model checked against the ABS

    A population's age and sex structure is drawn from counts, and its growth rate compounds, so a small annual percentage doubles a population within decades.

    Practical, model not builtLow risk
  42. Geography K–10 · Years 9–10

    Salinity and crops: a seedling trial checked against FAO salt-tolerance data

    Salt in soil water reduces plant growth once it passes a threshold that differs by crop, which is why land clearing that raises saline groundwater cuts food production.

    Practical, model not builtLow risk
  43. Geography K–10 · Years 9–10

    Soil texture by sedimentation: a jar test timed by Stokes' law

    A soil's sand, silt and clay fractions settle out of water at very different speeds because settling speed rises with the square of grain size, and the fractions decide how a soil holds water and supports a biome's productivity.

    Practical, model not builtLow risk
  44. Geography K–10 · Years 9–10

    Weed cover along a transect from a walking track into bushland

    Disturbance at a track edge lets weeds invade bushland, and point-intercept quadrats along a transect measure how weed cover changes with distance from the disturbance.

    PracticalMedium risk

For tutors and administrators

The materials and steps of every teacher-led demonstration are on the learning platform, with the safety card first. Sign in with a tutor or administrator account to read them.

Open the teacher-led demonstrations